File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

Book Chapter: Remote Sensing of the Land Surface Radiation Budget

TitleRemote Sensing of the Land Surface Radiation Budget
Authors
Liang, ShunlinZhang, XiaotongHe, TaoCheng, JieWang, Dongdong
Issue Date2014
PublisherTaylor & Francis
Citation
Remote Sensing of the Land Surface Radiation Budget. In Petropoulos, GP (Ed.), Remote Sensing of Energy Fluxes and Soil Moisture Content, p. 121-162. Boca Raton: Taylor & Francis, 2014 How to Cite?
DOI: http://dx.doi.org/10.1201/b15610-10
AbstractLand surface energy balance is central to characterizing land surface ecological, hydrological, and biogeochemical processes. The land surface energy balance equation can be written as Rn = G + H + λET (5.1) where Rn is the all-wave net radiation, G is the soil heat flux, H is the sensible heat flux, and λET is the latent heat flux in which λ is the latent heat of evaporation of water and ET is the rate of evaporation of water.
Persistent Identifierhttp://hdl.handle.net/10722/323163
ISBN
9781466505780

 

DC FieldValueLanguage
dc.contributor.authorLiang, Shunlin-
dc.contributor.authorZhang, Xiaotong-
dc.contributor.authorHe, Tao-
dc.contributor.authorCheng, Jie-
dc.contributor.authorWang, Dongdong-
dc.date.accessioned2022-11-18T11:55:09Z-
dc.date.available2022-11-18T11:55:09Z-
dc.date.issued2014-
dc.identifier.citationRemote Sensing of the Land Surface Radiation Budget. In Petropoulos, GP (Ed.), Remote Sensing of Energy Fluxes and Soil Moisture Content, p. 121-162. Boca Raton: Taylor & Francis, 2014-
dc.identifier.isbn9781466505780-
dc.identifier.urihttp://hdl.handle.net/10722/323163-
dc.description.abstractLand surface energy balance is central to characterizing land surface ecological, hydrological, and biogeochemical processes. The land surface energy balance equation can be written as Rn = G + H + λET (5.1) where Rn is the all-wave net radiation, G is the soil heat flux, H is the sensible heat flux, and λET is the latent heat flux in which λ is the latent heat of evaporation of water and ET is the rate of evaporation of water.-
dc.languageeng-
dc.publisherTaylor & Francis-
dc.relation.ispartofRemote Sensing of Energy Fluxes and Soil Moisture Content-
dc.titleRemote Sensing of the Land Surface Radiation Budget-
dc.typeBook_Chapter-
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1201/b15610-10-
dc.identifier.scopuseid_2-s2.0-85136876889-
dc.identifier.spage121-
dc.identifier.epage162-
dc.publisher.placeBoca Raton-

Export via OAI-PMH Interface in XML Formats

OR

Export to Other Non-XML Formats